The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are relatedTyndall, John
Science
The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are related
Tyndall, John
Alps -- Description and travel; Glaciers -- Alps
[Sidenote: LECTURE AT THE ROYAL INSTITUTION.]
The observations just referred to showed the co-existence of the two
phenomena, but they did not prove that pressure and cleavage stood to
each other in the relation of cause and effect. "Can the pressure
produce the cleavage?" was still an open question, and it was one which
mere reasoning, unaided by experiment, was incompetent to answer.
Sharpe despaired of an experimental solution, regarding our means as
inadequate, and our time on earth too short to produce the result. Mr.
Sorby was more hopeful. Submitting mixtures of gypsum and oxide of iron
scales to pressure, he found that the scales set themselves
approximately at right angles to the direction in which the pressure was
applied. The position of the scales resembled that of the plates of mica
which his researches had disclosed to him in slate rock, and he inferred
that the presence of such plates, and of flat or elongated fragments
generally, lying all in the same general direction, was the cause of
slaty cleavage. At the meeting of the British Association at Glasgow, in
1855, I had the pleasure of seeing some of Mr. Sorby's specimens, and,
though the cleavage they exhibited was very rough, still, the tendency
to yield at right angles to the direction in which the pressure had been
applied, appeared sufficiently manifest.
At the time now referred to I was engaged, and had been for a long time
previously, in examining the effects of pressure upon the magnetic
force, and, as far back as 1851, I had noticed that some of the bodies
which I had subjected to pressure exhibited a cleavage of surpassing
beauty and delicacy. The bearing of such facts upon the present question
now forcibly occurred to me. I followed up the observations; visited
slate yards and quarries, observed the exfoliation of rails, the fibres
of iron, the structure of tiles, pottery, and cheese, and had several
practical lessons in the manufacture of puff-paste and other laminated
confectionery. My observations, I thought, pointed to a theory of slaty
cleavage different from any previously given, and which, moreover,
referred a great number of apparently unrelated phenomena to a common
cause. On the 10th of June, 1856, I made them the subject of a Friday
evening's discourse at the Royal Institution.[B]
[Sidenote: ORIGIN OF RESEARCHES.]
Public-domain text, read in full here on John Shaqi.
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